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It has nothing to do with the surroundings and everything to do with the system. In the alternative reversible process, you need to add heat reversibly and isothermally to the system, so $$Q_{rev}=nRT\ln{(V_2/V_1)}$$and$$\Delta S=\frac{Q_{rev}}{T}=nR\ln{(V_2/V_1)}$$Philip Koeck said:I'll try to apply this idea to the free expansion of a gas, versus the reversible isothermal expansion.
In a free expansion the entropy change of the system is exactly the same as for a reversible isothermal expansion at the same temperature. The difference between the two processes seems to lie in what happens in the surroundings. This is what you see in summary, so to say.
In fact entropy is generated inside the system during the free expansion, whereas entropy flows from the surroundings to the system in a reversible isothermal expansion.
So, although the entropy change in the system has the same value for both processes they are fundamentally different.
Does that sound about right?
In the irreversible free expansion process between the same two states, $$Q=0$$and $$\Delta S=nR\ln{(V_2/V_1)}=\sigma+\frac{Q}{T}=\sigma$$where ##\sigma## is the entropy generated within the system during the irreversible free expansion as a result of viscous dissipation.
To give you a feel for how viscous dissipation comes into play in generating entropy, consider the following homework problem I've dreamed up for you: You have an incompressible viscous Newtonian fluid situated between two infinite insulated parallel plates in which the bottom plate is stationary and the upper plate is moving tangentially with constant velocity V. The velocity profile within the fluid between the plates is given by $$v=V\frac{y}{h}$$where h is the distance between the plates. The transient thermal energy balance on the fluid is given by$$\frac{dU}{dt}=\dot{W}$$ (where ##\dot{W}## is the rate at which the surroundings do work on the system), or, per unit volume, $$\rho C \frac{dT}{dt}=\mu\left(\frac{V}{h}\right)^2$$where ##\rho## is the fluid density, C is its heat capacity, and ##\mu## is its viscosity. If we assume that the fluid density, heat capacity, and viscosity are independent of temperature, and that the initial temperature (at time t = 0) is ##T_0##, what is the temperature at time T?
If we divide this heat balance equation by the temperature T, we obtain the entropy balance equation on the fluid. What is that entropy balance equation (in terms of the entropy per unit volume), and, by integrating that equation, what is the change in entropy per unit volume of the fluid between time t = 0 and time t?
I'll continue after you complete this.
Notice that we are doing all this without even looking at an alternative reversible path yet.
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